基于贝叶斯优化XGBoost-GIS协同模型的奥灰突水风险智能预测

Intelligent prediction of ordovician limestone water inrush risk based on bayesian optimized XGBoost-GIS synergistic model

  • 摘要: 针对深部煤矿开采过程中奥陶系灰岩承压含水层突水灾害预测存在的非线性、高复杂性建模难题,研究构建了一种融合贝叶斯优化(Bayesian Optimization, BO)与极限梯度提升(eXtreme Gradient Boosting, XGBoost)的智能预测模型(BO-XGBoost)。该模型以提升突水风险预测精度与可解释性为目标,研究范围涵盖水文地质参数非线性响应关系建模、关键致灾因子识别及空间风险可视化表达。采用BO算法对XGBoost的超参数进行全局寻优,克服传统调参方法效率低、易陷入局部最优的问题;模型通过迭代生成分类与回归树(CART),输出对数几率比,结合正则化与加权映射机制,将结果转换为0,1区间内的突水概率值,实现高精度分类预测,并将概率结果集成至地理信息系统(GIS)平台进行空间可视化,生成精细化风险分布图。试验结果表明:模型分类准确率达到85%,AUC值为0.83,显著优于BO-GBDT、BO-RF及标准XGBoost等对比算法。在司马煤矿的应用验证中,模型预测的突水概率场与传统突水系数法的空间结构相似性(SSIM)达71%,且通过概率阈值自适应划分风险等级,评估结果更具空间细节与区分度。基于SHAP(Shapley Additive Explanations)的可解释性分析显示,地质构造缺陷指数与隔水层等效厚度为突水主控因素,特征重要性分别为32.7%、28.4%,与岩体裂隙渗流理论一致。研究构建的BO-XGBoost-GIS协同模型实现了突水风险的高精度量化预测与机理可解释分析,为深部矿井奥陶系含水层突水防控提供了有效技术路径。

     

    Abstract: To address the nonlinear and highly complex modeling challenges in predicting water inrush disasters from Ordovician limestone confined aquifers during deep coal mining, this study develops an intelligent prediction model (BO-XGBoost) integrating Bayesian Optimization (BO) and eXtreme Gradient Boosting (XGBoost). The research aims to enhance prediction accuracy and model interpretability, covering the modeling of nonlinear hydrogeological responses, identification of key hazard-inducing factors, and spatial risk visualization. The BO algorithm is employed to globally optimize the hyperparameters of XGBoost, overcoming inefficiency and local optima issues inherent in traditional parameter tuning methods. The model iteratively generates Classification and Regression Trees (CART), outputs log-odds ratios, and through regularization and weighted mapping, transforms the results into water inrush probabilities within the 0,1 range, enabling high-precision classification. These probability outputs are then integrated into a Geographic Information System (GIS) platform for spatial visualization, generating refined risk distribution maps. Experimental results show that the model achieves a classification accuracy of 85% and an AUC value of 0.83, significantly outperforming comparative algorithms such as BO-GBDT, BO-RF, and standard XGBoost. Application and validation at Sima Coal Mine demonstrate a spatial structural similarity (SSIM) of 71% between the predicted water inrush probability field and the evaluation results from the traditional water inrush coefficient method. Risk levels are adaptively classified using probabilistic thresholds, yielding results with greater spatial detail and differentiation. SHAP (Shapley Additive Explanations) based interpretability analysis reveals that the geological structure defect index and the equivalent thickness of the aquiclude are the dominant factors influencing water inrush, with feature importances of 32.7% and 28.4%, respectively, consistent with rock mass fracture seepage theory. The developed BO-XGBoost-GIS collaborative model enables high-precision quantitative prediction and mechanistic interpretability of water inrush risk, providing an effective technical approach for water inrush prevention and control in deep coal mines with Ordovician aquifers.

     

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